Radar and Satellite Technology:
Radars
The word radar is an acronym from "Radio Detection and
Ranging". Radar images are useful for locating precipitation.
A radar sends a pulse
of energy into the atmosphere and if any precipitation is
intercepted by the energy, part of the energy is scattered
back to the radar. These returned signals, called "radar echoes", are
assembled to produce radar images.
Sending and Receiving Signals (detecting a target)

The
receiving antenna (which is normally also the transmitting antenna) gathers
this back-scattered radiation and feeds it to a device called a receiver.
The location of the colored radar echoes indicate where
precipitation is falling and the various colors indicate the intensity of the
precipitation through the color code in the lower left corner of the image.
Satellites:
A
satellite is defined as a man-made object put into orbit around a celestial
body, like the earth or the moon.
Satellites
serve a wide variety of purposes from transmission of television signals via
communication satellites to guidance and tracking systems of defense
satellites. For meteorologists, satellites provide a comprehensive view of the
world's weather. On April 1, 1960, the first weather satellite was launched
into orbit from the United States. Since then, weather satellites have been
launched into orbit and their capabilities have improved significantly. Satellites
carry imager
and sounder
instruments enabling them to image clouds,
monitor earth's surface
temperature and water vapor
fields, and sound the atmosphere for its vertical thermal and
vapor structures. Today, not only do satellites observe clouds, but
measure other non- visible radiation from the earth and atmosphere. This helps
us to estimate such aspects as crop and soil conditions.
Acknowledgement: The above information is taken from the following website:
Environment Canada's Radar and Satellite imagery:
Canadian Weather Radar
Satellite Images
http://www.weatheroffice.gc.ca/satellite/index_e.html
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